吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (2): 336-347.doi: 10.13278/j.cnki.jjuese.201602103
谭聪1, 于炳松1, 阮壮1, 刘策2, 朱玺3, 谢灏辰1, 罗忠2
Tan Cong1, Yu Bingsong1, Ruan Zhuang1, Liu Ce2, Zhu Xi3, Xie Haochen1, Luo Zhong2
摘要:
本文基于高分辨率层序地层学及沉积学的相关理论,以汭水河剖面、42口井的岩心资料以及97口井的测井资料为依据,对鄂尔多斯盆地西南部延长组进行了层序地层划分。结果显示,研究区内的延长组可划分为4个长期旋回,11个中期旋回。四次长期旋回的最大湖泛面位置分别对应于长9、长7、长4+5及长1油层组。研究发现盆地西南部地区延长组主要的旋回结构样式包括A/S小于1时,以上升半旋回为主的非对称结构;A/S接近1时,上升和下降旋回均保存完整的对称型结构及A/S大于1时,以下降半旋回为主的非对称结构。从南北向和东西向层序地层年代格架剖面分析可以发现,研究区内延长组内部不存在大型的或者区域性的沉积间断和不整合面,研究区延长组上部由于后期的构造抬升作用而被剥蚀,与上覆侏罗系呈假整合接触。
中图分类号:
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